Fig. 10From: Application of the on-site P-wave earthquake early warning method based on site-specific ratios of S-waves to P-waves to the 2016 Kumamoto earthquake sequence, JapanPredicted PGAs of S-waves using different time-window lengths from P-waves arrival for all the earthquakes at the strong-motion stations. In the figure, standard deviation σ and coefficient determination R2 in logarithm are indicated. Ndata indicates the number of earthquake datasets recorded at all the stationsBack to article page